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| title | chunk | source | category | tags | date_saved | instance |
|---|---|---|---|---|---|---|
| Bioarchaeology | 5/6 | https://en.wikipedia.org/wiki/Bioarchaeology | reference | science, encyclopedia | 2026-05-05T13:58:28.486766+00:00 | kb-cron |
The oxygen stable isotope system is based on the 18O/16O (δ18O) ratio in a given material, which is enriched/depleted relative to a standard. The field typically normalizes to both Vienna Standard Mean Ocean Water (VSMOW) and Standard Light Antarctic Precipitation (SLAP). This system is famous for its use in paleoclimatic studies but it also a prominent source of information in bioarchaeology. Variations in δ18O values in skeletal remains are directly related to the isotopic composition of the consumer's body water. isotopic composition of mammalian body water is primarily controlled by consumed water. δ18O values of freshwater drinking sources vary due to mass fractionations related to mechanisms of the global water cycle. Evaporated water vapor is more enriched in 16O (isotopically lighter; more negative delta value) compared to the remaining water, which is depleted in 16O (isotopically heavier; more positive delta value). An accepted first-order approximation for the isotopic composition of animal drinking water is local precipitation, though this is complicated to varying degrees by confounding water sources like natural springs or lakes. The baseline δ18O used in archaeological studies is modified depending on the relevant environmental and historical context. δ18O values of bioapatite in human skeletal remains are assumed to have formed in equilibrium with body water, thus providing a species-specific relationship to oxygen isotopic composition of body water. The same cannot be said for human bone collagen, as δ18O values in collagen seem to be impacted by drinking water, food water, and a combination of metabolic and physiological processes. δ18O values from bone minerals are essentially an averaged isotopic signature throughout the entire life of the individual. While carbon and nitrogen are used primarily to investigate the diets of ancient humans, oxygen isotopes offer insight into body water at different life stages. δ18O values are used to understand drinking behaviors, animal husbandry, and track mobility. 97 burials from the ancient Maya citadel of Tikal were studied using oxygen isotopes. Results from tooth enamel identified statistically different individuals, interpreted to be individuals from Maya lowlands, Guatemala, and potentially Mexico. Historical context combined with isotopic data from burials were used to argue that migrant individuals were a part of lower and higher social classes within Tikal. Female migrants who arrived in Tikal during Early Classic period could have been the brides of Maya elite.
==== Sulfur ==== The sulfur stable isotope system is based on small, mass-dependent fractionations of sulfur isotopes. These fractionations are reported relative to Canyon Diablo Troilite (V-CDT), the agreed upon standard. The ratio of the most abundant sulfur isotope, 32S, compared to rarer isotopes such as, 33S, 34S, and 36S, is used to characterize biological signatures and geological reservoirs. The fractionation of 34S (δ34S) is particularly useful since it is the most abundant of the rare isotopes. This system is less commonly used on its own and typically complements studies of carbon and nitrogen. In bioarchaeology, the sulfur system has been used to investigate paleodiets and spatial behaviors through the analysis of hair and bone collagen. Dietary proteins incorporated into living organisms tend to determine the stable isotope values of their organic tissues. Methionine and cysteine are the canonical sulfur-containing amino acids. Of the two, δ34S values of methionine are considered to better reflect isotopic compositions of dietary sulfur, since cysteine values are impacted by diet and internal cycling. While other stable isotope systems have significant trophic shifts, sulfur shows only a small shift (~0.5‰).
Consumers yield isotopic signatures that reflect the sulfur reservoir(s) of the dietary protein source. Animal proteins sourced from marine ecosystems tend to have δ34S values between +16 and +17‰, terrestrial plants range from -7‰ to +8‰, while proteins from freshwater and terrestrial ecosystems are highly variable. The sulfate content of the modern ocean is well-mixed with a δ34S of approximately +21‰, while riverine water is heavily influenced by sulfur-bearing minerals in surrounding bedrock and terrestrial plants are influenced by the sulfur content of local soils. Estuarian ecosystems have increased complexity due to seawater and river inputs. The extreme range of δ34S values for freshwater ecosystems often interferes with terrestrial signals, making it difficult to use the sulfur system as the sole tool in paleodiet studies. Various studies have analyzed the isotopic ratios of sulfur in mummified hair. Hair is a good candidate for sulfur studies as it typically contains at least 5% elemental sulfur. One study incorporated sulfur isotope ratios into their paleodietary investigation of four mummified child victims of Incan sacrificial practices. δ34S values helped them conclude that the children had not been eating marine protein before their death. Historical insight coupled with consistent sulfur signatures for three of the children suggests that they were living in the same location 6 months prior to the sacrifice. Studies have measured δ34S values of bone collagen, though the interpretation of these values was not reliable until quality criteria were published in 2009. Though bone collagen is abundant in skeletal remains, less than 1% of the tissue is made of sulfur, making it imperative that these studies carefully assess the meaning of bone collagen δ34S values.
== DNA == DNA analysis of past populations is used to genetically determine sex, determine genetic relatedness, understand marriage patterns, and investigate prehistoric migration. In 2012 archaeologists found skeletal remains of an adult male. He was buried under a car park in England. DNA evidence allowed the archaeologists to confirm that the remains belonged to Richard III, the former king of England who died in the Battle of Bosworth. In 2021, Canadian researchers analyzed skeletal remains found on King William Island, identifying them as belonging to Warrant Officer John Gregory, an engineer serving aboard HMS Erebus in the ill-fated 1845 Franklin Expedition. He was the first expedition member to be identified by DNA analysis.